0000000000465563

AUTHOR

Robert Herman Wagner

showing 3 related works from this author

Revision and significance of the Westphalian (Middle Pennsylvanian) arborescent lycopsid Bergeria dilatata (Lindley &Hutton) Alvarez Vázquez & Wagner

2018

Wagner ArtículoRevision and significance of the Westphalian (Middle Pennsylvanian) arborescent lycopsid Bergeria dilatata (Lindley &ampUNESCO::CIENCIES DE LA VIDA:CIENCIES DE LA VIDA [UNESCO]Revision and significance of the Westphalian (Middle Pennsylvanian) arborescent lycopsid Bergeria dilatata (Lindley &Hutton) Alvarez Vázquez & Wagner ArtículoHutton) Alvarez Vázquez &amp
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The extrabasinal elements in Lower Pennsylvanian floras of the Maritime Provinces, Canada: Description of Adiantites, Pseudadiantites and Rhacopterid…

2021

Adiantites adiantoide s (Lindley and Hutton) Kidston, Pseudadiantites sessilis (Roehl) Gothan and Pseudadiantites rhomboideus (Ettingshausen) comb. nov. are figured and described as well as Rhacopteridium speciosum (Ettingshausen) Hirmer, as part of a revision of lower Pennsylvanian floras of Nova Scotia. These species show a foliar branching structure which is described as "pseudopinnate" as against the fully planated pinnate structure of the Palaeozoic fern and pteridosperm fronds. Their systematic affinity is unknown. A discussion is presented of the genera A diantites, Pseudadiantites, Aneimites , Palaeopteridium , and Triphyllopteris , and the problematic nature of the history of Adian…

Nova scotiaFrondPaleozoicbiologyPaleontologybiology.organism_classificationQE701-760PaleontologyGeographyHabitatPennsylvanianFernflora pennsylvanian namurian westphalian nova scotia extrabasinal.PalaeogeographySpanish Journal of Palaeontology
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SIGNIFICANCE FOR INTERNATIONAL CORRELATION OF THE PERAPERTÚ FORMATION IN NORTHERN PALENCIA, CANTABRIAN MOUNTAINS. TECTONIC/STRATIGRAPHIC CONTEXT AND …

2021

Small ammonoid assemblages are recorded from the Perapertú Formation in northern Palencia. This is a mudstone unit with local platform limestones characterised by carbonate debris flows on the limestone margins. This unit, of Late Bashkirian to Early Moscovian age, participates in a series of southwards verging thrust slicesNorth of a major fault zone which originated as the head (leading edge) of a large thrust sheet with an internal deformation consisting of thrust slices and at least one nappe structure. Opposed vergencies at the head of this major thrust sheet (Carrionas Thrust Front) and the Ruesga Fault which locally modifies its trace, mark the position where the northern branch of t…

geographygeography.geographical_feature_categorybiologyammonoids carboniferous bashkirian moscovian westphalian palentian domain cantabrian mountains tectonics.GoniatitesPaleontologyContext (language use)Fold (geology)Fault (geology)biology.organism_classificationQE701-760Westphalian sovereigntyNappePaleontologyGoniatiteCarboniferousCartographySpanish Journal of Palaeontology
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